Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments

Mediterranean-climate catchments are characterized by significant spatial and temporal hydrological variability caused by the interaction of natural as well human-induced abiotic and biotic factors. This study investigates the non-linearity of rainfall-runoff relationship at multiple temporal scales...

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Main Authors: Josep Fortesa, Jérôme Latron, Julián García-Comendador, Miquel Tomàs-Burguera, Jaume Company, Aleix Calsamiglia, Joan Estrany
Format: Article
Language:English
Published: MDPI AG 2020-01-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/12/1/299
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spelling doaj-5be984f32a5d40d2826c41a0a7281e752020-11-25T02:20:25ZengMDPI AGWater2073-44412020-01-0112129910.3390/w12010299w12010299Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate CatchmentsJosep Fortesa0Jérôme Latron1Julián García-Comendador2Miquel Tomàs-Burguera3Jaume Company4Aleix Calsamiglia5Joan Estrany6Mediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainInstitute of Environmental Assessment and Water Research (IDAEA), Spanish Research Council (CSIC), Jordi Girona 18, 08034 Barcelona, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainEstación Experimental de Aula Dei, Consejo Superior de Investigaciones Científicas (EEAD-CSIC), 50192 Zaragoza, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainMediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of Geography, University of the Balearic Islands, Ctra. Valldemossa km 7.5, 07122 Palma, Balearic Islands, SpainMediterranean-climate catchments are characterized by significant spatial and temporal hydrological variability caused by the interaction of natural as well human-induced abiotic and biotic factors. This study investigates the non-linearity of rainfall-runoff relationship at multiple temporal scales in representative small Mediterranean-climate catchments (i.e., &lt;10 km<sup>2</sup>) to achieve a better understanding of their hydrological response. The rainfall-runoff relationship was evaluated in 43 catchments at annual and event&#8212;203 events in 12 of these 43 catchments&#8212;scales. A linear rainfall-runoff relationship was observed at an annual scale, with a higher scatter in pervious (R<sup>2</sup>: 0.47) than impervious catchments (R<sup>2</sup>: 0.82). Larger scattering was observed at the event scale, although pervious lithology and agricultural land use promoted significant rainfall-runoff linear relations in winter and spring. These relationships were particularly analysed during five hydrological years in the Es Fangar catchment (3.35 km<sup>2</sup>; Mallorca, Spain) as a temporal downscaling to assess the intra-annual variability, elucidating whether antecedent wetness conditions played a significant role in runoff generation. The assessment of rainfall-runoff relationships under contrasted lithology, land use and seasonality is a useful approach to improve the hydrological modelling of global change scenarios in small catchments where the linearity and non-linearity of the hydrological response&#8212;at multiple temporal scales&#8212;can inherently co-exist in Mediterranean-climate catchments.https://www.mdpi.com/2073-4441/12/1/299rainfall-runoffmultiple temporal scalesnon-linearitysmall catchmentsmediterranean
collection DOAJ
language English
format Article
sources DOAJ
author Josep Fortesa
Jérôme Latron
Julián García-Comendador
Miquel Tomàs-Burguera
Jaume Company
Aleix Calsamiglia
Joan Estrany
spellingShingle Josep Fortesa
Jérôme Latron
Julián García-Comendador
Miquel Tomàs-Burguera
Jaume Company
Aleix Calsamiglia
Joan Estrany
Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments
Water
rainfall-runoff
multiple temporal scales
non-linearity
small catchments
mediterranean
author_facet Josep Fortesa
Jérôme Latron
Julián García-Comendador
Miquel Tomàs-Burguera
Jaume Company
Aleix Calsamiglia
Joan Estrany
author_sort Josep Fortesa
title Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments
title_short Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments
title_full Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments
title_fullStr Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments
title_full_unstemmed Multiple Temporal Scales Assessment in the Hydrological Response of Small Mediterranean-Climate Catchments
title_sort multiple temporal scales assessment in the hydrological response of small mediterranean-climate catchments
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2020-01-01
description Mediterranean-climate catchments are characterized by significant spatial and temporal hydrological variability caused by the interaction of natural as well human-induced abiotic and biotic factors. This study investigates the non-linearity of rainfall-runoff relationship at multiple temporal scales in representative small Mediterranean-climate catchments (i.e., &lt;10 km<sup>2</sup>) to achieve a better understanding of their hydrological response. The rainfall-runoff relationship was evaluated in 43 catchments at annual and event&#8212;203 events in 12 of these 43 catchments&#8212;scales. A linear rainfall-runoff relationship was observed at an annual scale, with a higher scatter in pervious (R<sup>2</sup>: 0.47) than impervious catchments (R<sup>2</sup>: 0.82). Larger scattering was observed at the event scale, although pervious lithology and agricultural land use promoted significant rainfall-runoff linear relations in winter and spring. These relationships were particularly analysed during five hydrological years in the Es Fangar catchment (3.35 km<sup>2</sup>; Mallorca, Spain) as a temporal downscaling to assess the intra-annual variability, elucidating whether antecedent wetness conditions played a significant role in runoff generation. The assessment of rainfall-runoff relationships under contrasted lithology, land use and seasonality is a useful approach to improve the hydrological modelling of global change scenarios in small catchments where the linearity and non-linearity of the hydrological response&#8212;at multiple temporal scales&#8212;can inherently co-exist in Mediterranean-climate catchments.
topic rainfall-runoff
multiple temporal scales
non-linearity
small catchments
mediterranean
url https://www.mdpi.com/2073-4441/12/1/299
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